Ice-proximal glaciofluvial gravels at Howe of Byth, Grampian Region, h
ave given luminescence ages of 45 +/- 4 and 37 +/- 4 ka BP. The gravel
s were laid down by meltwater draining from an ice margin in the Moray
Firth and provide the first firm evidence of extensive glaciation in
NE Scotland during the Mid Devensian.